Science

Microbe found in Ethiopian volcano in 192°F waters hints at life on Mars' harsh conditions


Microbe found in Ethiopian volcano that survives in 192°F waters hints that life on Mars may be able to withstand the harsh environment on the planet

  • The microbe lives in extremely saturated salt water that are highly acidic
  • In the hottest inhabited place on Earth in a volcanic thermal spring in Ethiopia 
  • Such conditions are similar to environments on early Mars, scientists say
  • And can reveal more about our own plant as well as life on the Red Planet 

A tiny microbe has been discovered that can survive in conditions similar to the extreme environments found on Mars, say scientists.

It lives in one of the hottest places on Earth in supersaturated salt water that are 89°C (192°F) and strongly acidic.

The bacteria is the first evidence of a living species able to survive in the hot springs of the region.

Its similarities to the thermal environments of early Mars could reveal more secrets about Earth and the origins of the Red Planet, experts say.

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A super tiny microbe has been discovered that can survive in conditions similar to the extreme early environments on Mars, say scientist. Dallol is a hydrothermal field located in the northern Danakil Depression, despite being known as Dallol Volcano

WHAT IS THE GUSEV CRATER? 

Gusev Crater, a 90-mile (145km) wide hole in the surface of Mars that probably formed three to four billion years ago when an asteroid crashed just south of the planet’s equator.

Scientists believe that the crater was covered by standing water, maybe in the form of a lake, early in the history of Mars. 

There’s a channel system that drains into it, which probably carried liquid water, or water and ice, into the crater.

Inside the crater, researchers expect to find sediments, which may be nearly 3,000 feet (915 metres) thick.

These sediments, which, researchers hope were deposited by water, may have been covered by dust and sand that’s blown into the crater over the past two billion years.

But if there was once water in Gusev, its signature should still be there.

Dallol hydrothermal field in the Danakil depression in Ethiopia – where the research took place – is the hottest inhabited place in the world and home to a technicoloured landscape of yellows, reds, greens and blues. 

Located at the northern end of the Danakil Depression the area has an average annual temperatures of are 36 to 38°C (97 to 100°F). 

‘This is an exotic, multi-extreme environment, with organisms that need to love high temperature, high salt content and very low pH in order to survive,’ said Dr Dr Felipe Gómez from the Astrobiology Center in Spain.

The unusual geochemistry of Dallol has close parallels to hydrothermal environments found on Mars, including the Gusev Crater, where NASA’s Spirit Mars Exploration Rover landed.

Spirit was robotic rover on Mars, active from 2004 to 2010. 

It was sent to explore Mars and search for signs of past life and found evidence that Mars was once much wetter than it is today.

Dallol’s distinctive ridges were created by rainfall that contains superheated water saturated with salts such as silver chloride, zinc iron sulphide, manganese dioxide and normal rock-salt. 

The bacteria lives in one of the hottest places on earth in super saturated salt water that are 192°F (89 degrees Celsius) and strongly acidic. This map shows Dallol's location in north-east Ethiopia - an area known for its extreme environment

The bacteria lives in one of the hottest places on earth in super saturated salt water that are 192°F (89 degrees Celsius) and strongly acidic. This map shows Dallol’s location in north-east Ethiopia – an area known for its extreme environment

The bacteria is the first evidence of a living species able to survive in the hot thermal waters of the Dallol region (pictured)  in the Danakil Depression

The bacteria is the first evidence of a living species able to survive in the hot thermal waters of the Dallol region (pictured)  in the Danakil Depression 

The volcanic activity heats the water which is enriched in gases from a magma reservoir beneath the volcano. 

A team of researchers collected samples from the Dallol volcano from a thin layers of salt deposits that came from supersaturated water with the extremely acidic pH of 0.25.

These were extracted from the hotsprings from the wall of a yellow chimney stack and a blue pool of water surrounding it. 

The salt samples were then transported to analysed using methods including electron microscopy, chemical analysis and DNA sequencing in Spain.

Their analysis identified tiny, spherical structures within the salts that had a high carbon content, confirming the presence of a biological species.

The species found in the salt deposits at Dallol was a strain of the Nanohaloarchaeles Order bacteri (pictured) that can survive extreme temperatures including high salt saturation and acidic levels

The species found in the salt deposits at Dallol was a strain of the Nanohaloarchaeles Order bacteri (pictured) that can survive extreme temperatures including high salt saturation and acidic levels

The species was found to be a strain of the Nanohaloarchaeles Order bacteria.  

Researchers wrote in the report: ‘The results from this study suggest the microorganisms can survive, and potential live, within this extreme environment, which has implications for understanding the limits of habitability on Earth and on (early) Mars.’

Barbara Cavalazzi of the University of Bologna, lead author of the review, added: ‘Deep investigation of the characteristics of this amazing site will improve our understanding of the limits of life on Earth an inform our search for life on Mars and elsewhere in the Universe.’

The full report was published in the journal Scientific Reports

WHERE IS THE DANAKIL DEPRESSION?

Ethiopia’s Danakil depression  is the hottest inhabited place on Earth and home to the Dallol sulfur springs in its north, which astrobiologists are studying to investigate how life on other planets could form under such harsh conditions. 

The Dallol Volcano, in Ethiopia, is an endless yellow-orange landscape, its craters stretching for miles around. 

The area has an average annual temperatures of are 36 to 38°C (97 to 100°F). 

The craters were formed by the intrusion of magma in salt deposits and hydrothermal activity.

The volcanic activity heats the water which is enriched in gases from a magma reservoir beneath the volcano.  

The thermal craters contain extremely saturated salt water that are 89°C (192°F) and strongly acidic with a ph of 0.25. 

Its similarities to the thermal environments of early Mars could reveal more secrets about Earth and the origins of the Red Planet, experts say. 



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